La Caliza de Peña Redonda (Westfaliense A-B):: Evolución tecto-sedimentaria (Cuenca Carbonífera Central asturiana).

• Autores: Carlos Ignacio Salvador González
• Localización: Geogaceta, ISSN 0213-683X, Nº. 9, 1990, págs. 53-56
• Idioma: español
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• Resumen

  • The occurrence of destructive carbonatic facies at the top of a tectonically controlled megasequence and his probable widespread distribution may be an indicator of an extensive emersion during Westfalian A-B boundary, and could hide important changes in the local fossil distribution